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Seismology is the study of earthquakes, which occur when stress causes rocks under the Earth's crust to elastically deform until they break, rebounding and snapping back into their original shape. This elastic rebound releases energy in the form of seismic waves, causing the shaking that defines an earthquake. Faults form from tectonic stresses and are breaks in the Earth's crust. The focus is the point within the earth where an earthquake originates, while the epicenter is the point on the surface directly above the focus.





